Long-range transport of iron via the Agulhas Current and counter-current: a boon for the phytoplankton

Bucciarelli, Penven et al. (2025, see reference below) combined float trajectories with high-resolution model diagnostics, thus could establish that a significant iron fertilisation was explaining the huge phytoplankton bloom recurrently observed in the western Indian Subantarctic Zone. They show that the energetic Agulhas current is leaching sedimented iron over the African margin, crossing the Subtropical Front via the region’s intense mesoscale eddy variability with the Agulhas Return Current (ARC), eventually transporting iron through the Sub Tropical Front (STF) and extending into the Sub Antarctic Zone (SAZ). So far, it was established that aeolian inputs to this area support only about half of the biological iron demand in the SAZ. The results of Bucciarelli, Penven et al. contribute to balance the dissolved iron budget for this region, which productivity represents 20–40% of Southern Ocean carbon export to the deep ocean. Beyond the present fertilisation, the authors also hypothesised that the past ARC variability could have influenced past productivity across much of the western Indian SAZ, providing a convincing reconstruction over the past 350 ka.

Figure: Satellite chlorophyll-a for the 25/12/2017 mapped on ocean surface topography shows the Agulhas Front (AF), Subtropical Front (STF) and Subantarctic Front (SAF). Purple lines trace floats passing near the East African margin (black triangles), about half of which cross the STF. These waters carry Fe from the African margin into the SAZ, supplying half of the phytoplankton’s iron needs. The inset indicates that past changes in the strength of the Agulhas Return Current over the last 350 kyr (a) may have influenced productivity in the western Indian SAZ (c-e), alongside variations in dust inputs (b).

Reference:

Bucciarelli, E., Penven, P., Pous, S., & Tagliabue, A. (2025). Western Indian subantarctic phytoplankton blooms fertilized by iron-enriched Agulhas water. Nature Geoscience, 18, 1152–1158. Access the paper:10.1038/s41561-025-01823-z

Read also the “Behind the paper” post: https://communities.springernature.com/posts/the-southern-agulhas-leakage-a-source-of-iron-for-the-southern-ocean?channel_id=behind-the-paper

Latest highlights

Continuous record of the Antarctic Circumpolar Current latitude over the last glacial-interglacial cycles

The meridional positions of the oceanic fronts separating subtropical and Antarctic waters are key to constraining the mechanisms that drive the degassing of deeply-stored CO2 at the end of the glacial periods…

23 Million Years of iron sources reconstructed in the Northwest Pacific Ocean using iron isotopes in a ferromanganese crust

Using iron isotopes and elemental records, Chu and co-workers analysed an iron-manganese crust recovered from the Hongyan Seamount, and reconstructed the sources of dissolved Fe to the Northwest Pacific Ocean…

Variability of the past deep-water masses in the Arabian Sea over the last 41ka

Shukla and colleagues propose a high-resolution authigenic ƐNd record measured from a sediment core located in the eastern Arabian Sea…

Arctic outflows to Davis Strait and the Labrador Sea traced by radionuclide distributions

This study demonstrates that Arctic outflows through the Canadian Arctic Archipelago play a much more significant role than previously recognised.

Rechercher